The genesis of the Hashitu porphyry molybdenum deposit, Inner Mongolia, NE China: constraints from mineralogical, fluid inclusion, and multiple isotope (H, O, S, Mo, Pb) studies-Reference-Cited by-同舟云学术

The genesis of the Hashitu porphyry molybdenum deposit, Inner Mongolia, NE China: constraints from mineralogical, fluid inclusion, and multiple isotope (H, O, S, Mo, Pb) studies

Published:2017-06-17 Issue:3 Volume:53 Page:377-397
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Zhai Degao,Liu Jiajun,Tombros Stylianos,Williams-Jones Anthony E.

Funder

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/article/10.1007/s00126-017-0745-5/fulltext.html

Reference85 articles.

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2. Arnold GL, Anbar AD, Barling J, Lyons TW (2004) Molybdenum isotope evidence for widespread anoxia in mid-Proterozoic oceans. Science 304:87–90

3. Audétat A (2015) Compositional evolution and formation conditions of magmas and fluids related to porphyry Mo mineralization at Climax, Colorado. J Petrol 56:1519–1546

4. Bodnar RJ, Burnham CW, Sterner SM (1985) Synthetic fluid inclusions in natural quartz. III. Determination of phase equilibrium properties in the system H2O-NaCl to 1000 °C and 1500 bars. Geochim Cosmochim Acta 49:1861–1873

5. Brown PE, Lamb WE (1989) P-V-T properties of fluids in the system NaCl ± H2O ± CO2: new graphical presentations and implications for fluid inclusions studies. Geochim Cosmochim Acta 53:1209–1221

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